JEQ Journal of Natural Resources and Life Sciences Education
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Published in J Environ Qual 14:314-323 (1985)
© 1985 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
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Biogeochemistry of Aluminum in McDonalds Branch Watershed, New Jersey Pine Barrens1

R. S. Turner, A. H. Johnson and D. Wang2

ABSTRACT

Aluminum concentrations, fluxes, and storage were measured in the vegetation, forest floor, and acid, sandy mineral soil of a forested watershed in the New Jersey Pine Barrens. Volume-weighted mean Al concentrations in solution increased as water passed through the upland ecosystem, from 0.012 mg L–1 in bulk precipitation to 0.14 mg L–1 in throughfall to 0.45 mg L–1 in E horizon mineral soil, 0.60 mg L–1 in the B horizon, and 0.73 mg L–1 in the C horizon. Weighted mean Al concentration of the stream water was 0.15 mg L–1. Solution Al concentrations in different compartments of the ecosystem were related to the magnitude of moisture flux, dissolved organic carbon concentration, and pH. Soil solution and stream water Al concentrations were high in the winter and spring and low in the summer and fall, inversely following solution pH. Soil solution and stream pH were independent of precipitation pH because of internal control of H+ concentration by the soil and an apparent 0.5-yr time lag in flushing of atmospherically deposited acids through the soil. Aluminum was partitioned strongly into the lower mineral soil horizons, but large stores of potentially labile Al were found in the upper mineral horizons and forest floor. Standing vegetation represented a relatively small pool of Al but cycled substantial amounts of Al between mineral soil and the forest floor.

Key Words: acid precipitation • budgets • forest soils • lysimeters


NOTES

1 Contribution from the Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN operated by Martin Marietta Energy Systems, Inc. under contract DE-ACO5-840R21400 with the U.S. Dep. of Energy, Environmental Sciences Division, Publication no. 2489; Dep. of Geology, Univ. of Pennsylvania, Philadelphia, PA 19104 and School of Forestry & Environmental Studies, Yale Univ., New Haven, CT 06511. This research was funded in part by grants from the Andrew W. Mellon Foundation, the Surdna Foundation, and the EPA/NCSU Acid Precipitation Program (a cooperative agreement between the U.S. Environmental Protection Agency and North Carolina State Univ.). It has not been subjected to EPA's required peer and policy review and therefore does not necessarily reflect the views of the Agency and no official endorsement should be inferred.

2 Research associate, Oak Ridge National Laboratory, Oak Ridge, TN 37831, associate professor, Univ. of Pennsylvania, Philadelphia, PA 19104, and associate in research, Yale Univ., New Haven, CT 06511, respectively.

Received for publication December 3, 1982.





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Copyright © 1985 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.